SOIL PROPERTIES A crash course in soils
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Transcript of SOIL PROPERTIES A crash course in soils
SOIL PROPERTIESA crash course in soils
D. SmithRaleigh Charter H.S.
2005-06
What is Soil?? Soil is the top layer of the Earth’s surface. Soils are the transition between the biotic
and abiotic worlds. Soil is a mixture of:
1. Minerals 2. Water3. Gases4. HUMUS-Dead “things” that have broken down
and become organic material—decayed plant and animal remains
(thanks to decomposing fungi and bacteria)
Soil Composition Mineral matter
comes from parent material
Air & Water percents are interchangeable
Humus is organic matter!
Water (~25%)
Air (~25%)
Mineral(~45%)
Humus (~5%)
Soils are important:◦ As a habitat for growing crops
Food Fabrics/Dyes Rubber/Building Materials
◦ As foundations of buildings◦ As beds for roads and highways◦ As an absorbent of domestic wastes in rural
areas as well as a depository for other wastes◦ As a filter for pollution that comes from rain and
water runoff◦ Medium for photosynthesis
Why are soils important?
There are THREE main contributing factors
1. The materials (rocks) from which they form- these are called PARENT MATERIAL
2. The ENVIRONMENT in which they developed (climate, vegetation, soil life, topography)
3. Length of time soils have been developing—the AGE of the soils
Good rule of thumb: 500-1000 yrs per inch of topsoil
How does soil form?
Mineral Matter◦ Provides nutrient minerals
for plants◦ Provides pore space for
water & air
Older soils are:◦ More weathered◦ Lower in certain
essential nutrient minerals
Soil Composition continued…
Humus: black/dark brown organic material remaining after
decomposition– Leaf litter, animal dung, & decaying organisms– Increases the soil’s water-holding capacity by
acting like a sponge
WEATHERING: Any process where rock breaks down (changes chemically and physically)
There are two types of weathering:Physical or Mechanical Weathering: Large
rock mass is broken into smaller fragments of the same type-NO CHEMICAL CHANGE
Chemical Weathering: mass of rock is decomposed by chemical reactions
How do parent materials get into soils??
Followed by Erosion (Wind, Water, Ice) What are “agents” of physical weathering?
◦ Tree roots/plant roots◦ Frost wedging:
1. Water collects in cracks in rock2. Water expands when it freezes3. Pieces of rock break off
Physical Weathering
Let’s take a closer look at frost wedging…
1.Water collects in cracks in rock
2.Water expands when it freezes
3.Water melts; Pieces of rock break off
Rock
Most chemical weathering involves gases in the atmosphere (oxygen and carbon dioxide) and/or water
Example: Think about metal rusting◦You go from metal to rust—a chemical reaction has taken place
Chemical Weathering
Topsoil Formation
Detritus-based Soil Ecosystem
All these happy little critters break down dead plant and animal
material and aerate the soil—they make topsoil!
Earthworms & Ants: ◦ Cycle minerals◦ Aerate the soil◦ Decomposing corpses
contribute organic matter◦ Assist plants in
reproduction by burying seeds
Mycorrhizae◦ Symbiotic relationship
between fungi and the roots of vascular plants
◦ Fungus absorbs nutrients from the soil, and provides it for the plant.
◦ Plant produces food (photosynthesis), and provides it for the fungus.
Soil Food Web
Soil Food Web (incl. humans)
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Texture pH Permeability Porosity Nutrient Levels—Nitrogen/Phosphorus
What are some soil properties?
Soil texture: The way a soil "feels"◦ Depends on the fraction each size of
particle in the soil◦ Sand, silt, and clay are names that
describe the size of individual particles in the soil. SAND are the largest particles and they feel
"gritty.“ SILT are medium sized, and they feel soft,
silky or "floury" CLAY are the smallest sized particles, and
they feel "sticky" and they are hard to squeeze.
SOIL TEXTURE
Texture is determined by its % sand, silt, and clay.
Texture determines the type of soil, and the soil’s properties.
Physical Property: Texture
Loam: ideal for
agricultural soil
Predicts soil properties-fertility, etc. Sandy soils
low organic matterPoor retention water and nutrients (it flows through)
As silt and clay fractions increase, soilsMore organic matterBetter bufferedBetter retention of water and nutrients
But you can have TOO much clayHard to cultivate-too sticky when wet; too hard when dryShrinks and swells
The best soils are a mix of all three and are called LOAM
Why care about soil texture?
Check-InSOIL PROPERTY
DEF. WHY CARE?
OTHER INFO
Texture Way a soil feels; Based on sand, silt, and clay amounts
Determines many soil properties; how workable; holding capacity
Sand = largest, silt = middle, clay = smallest;SAND—bad holding capacity; low OM; workable; CLAY- great holding; but shrink/swell; LOAM = 1/3 mix—BEST!!
Physical: Porosity & Permeability again… Think it is important??
Definition?◦ amt of soil pore spaces (aeration)
Porosity
PermeabilityDefinition?
– ability of water to percolate through
____ porosity = ____ permeability
Soil Composition continued…
As water infiltrates the soil, it can carry dissolved materials with it.
Leaching: Removal of dissolved materials from the soil by water percolating downward
Illuviation: Deposition of leached material in lower layers◦ Some substances completely leach out of the
soil because they’re so soluble that they migrate right down to the groundwater.
Physical: Ionic Charge Soil minerals are often present as ions. Minerals ions are either positively or
negatively charged. Clay particles have mostly negative
charges on their outer surfaces.◦Positively charged mineral ions are
attracted to the soil particles and are held for plant use. potassium K+ and magnesium Mg2+
◦Negatively charged mineral ions are repelled by the soil particles and are washed away from roots. nitrate NO3
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Physical Characteristics (review)
Why would 100% sand be undesirable for plants? Why would 100% clay be undesirable for plants? Answer SAND / SILT / CLAY for the following:
◦ A soil with a lot of _____ would have good drainage, but poor nutrient-holding characteristics.
◦ A soil with a lot of _____ would have poor drainage, but good nutrient-holding characteristics.
◦ A soil with a lot of _____ would have low porosity.◦ A soil with a lot of _____ would have high permeability.
Chemical Property: pH
Most soil pH is 4-8. Plants are happiest at 6-7. Plants are affected by soil pH.
(1) The solubility of certain nutrient minerals varies with differences in pH Low pH = Al & Mn are more soluble, and can be absorbed in toxic
amounts. High pH = some salts are less soluble, and are less available to the
plants.(2) Soil pH affects the leaching of nutrient minerals.
Acidic soil = positively charged ions are less soluble and are unavailable for plants.
PESTICIDE TIE-IN: If soil is too acidic, applied pesticides, herbicides, and fungicides will not be absorbed (held in the soil) and they will end up in runoff
Plant pH PreferencesPlants the like
strongly acid soil (pH 4.0 to 4.0)
Plants that prefer slightly acid soil (pH 5.0 to 6.5)
Plants that prefer neutral soil
(pH 6.0-8.0)
• Sundew• Pitcher Plants• Venus flytrap• Azalea• Rhododendron• Camellia
• American holly• Orchids• Many evergreen
trees and shrubs• Strawberries• Potatoes• Carrots• Fescue grasses
• Alfalfa• Bluegrass• Most vegetables (lettuce, tomato)• Grains (corn,
wheat)
Soil Conditioners (Lime) CaCO3 or MgCO3 Soil amendment / conditioner… not a
fertilizer! Important functions:
1. Corrects soil acidity2. Adds important plant nutrients— Ca & Mg3. Reduces solubility & toxicity of certain elements
in the soil Al, Mn, FeThis toxicity could reduce plant growth under acid conditions.
4. Promotes availability of major plant nutrients. Zn, Cu, P
5. Increases bacterial activity & mutualistic relationships.
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Soil stores important nutrients
http://www.lesco.com/
Phosphorus (P)Nitrogen (N)
Potassium (K)Calcium (Ca)
Magnesium (Mg)
Dr. Greg Pillar, Queens College
Nitrogen
Phosphorus
Soil Nutrients• Nutrients: essential chemical elements needed for
the growth of healthy plants
• Plants get nutrients from soil after the nutrients have dissolved in the soil solution (the water around soil particles)
• Each nutrient has specific roles in producing healthy plants
FUNCTIONS Used to make chlorophyll Responsible for rapid growth and health
green leavesTOO LITTLE/TOO MUCH Not enough nitrogen? Plant leaves turn yellow Too much nitrogen?
Long weak stems/no floweringMOVEMENT THROUGH and TO THE
SOIL: Nitrogen Cycle
NITROGEN
FUNCTION Responsible for root development and growth Helps plant produce flowers and fruit Important in photosynthesis and respiration, energy
transfer and storageTOO MUCH/TOO LITTLE Not enough phosphorus?
Purplish or deep green leaves Poor root system
Too much phosphorus? No symptoms Plants NEVER have too much phosphorus—there’s not a lot out there—what does exist bonds to soil or leaches away quickly
MOVEMENT THROUGH and TO THE SOIL: Phosphorus cycle
PHOSPHORUS
What is a soil profile?
Picturing a Soil ProfileImagine a hill…
Imagine the bulldozer taking a good chunk out of that hill.Hey, look at all the layers! That’s the soil profile…
Imagine a bulldozer…Layers are called horizons
Soil Profiles◦ the sequence of layers (horizons) from the surface downward
to rock or other underlying material Soil Layers “O”- organic horizons, litter derived from dead
plants andanimals
A- eluvial, mineral horizons which lie at or near thesurface and are characterized as zones of maximumleaching (E = Exit)
B- illuvial, washed in, layer of accumulation (I = Into)
C- unconsolidated material under A&B layers Bedrock
Soil Profiles
Soil profile example
Maryland Soil Profile
Soil Profile Example 2
Florida Soil Profile
Some Review Questions
• What effect does temperature have on soil?– It controls how fast organic material breaks down
• How might pH affect soil?– It changes what nutrients are available and toxins
(e.g. metals) in the soil• What is a soil profile?
– The cross-section of soil that shows different layers